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Stream length ratio (R L) considered as an important factor in relation to both drainage composition and geomorphic development of watersheds was also computed.
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The factors responsible for the development of watershed system are identified.
Length of overland flow (Lg) is one of the most important independent variables affecting the development of watershed.
This calls for sustainable development of watershed in terms of surface and ground water resources in this area.
Using the LPS method for sensor geometry modeling the extraction of the corresponding DEM produced good results that are suitable for the operational use in planning and development of natural watersheds.
Human development of coastal watersheds has greatly accelerated environmental pressure on downstream estuarine and coastal ecosystems; yet, unfortunately, assessing detrimental changes in these systems is complex.
The rho coefficient signifies the storage capacity of a watershed and determines the relationship between drainage density and physiographic development of the watershed.
It is used to determine the geomorphic stages of development of a watershed and expresses simply how the mass is distributed within a watershed from base to top. Figure 5 illustrates the definition of two dimensionless variables involved in hypsometric analysis.
The Rho coefficient is an important parameter relating drainage density to physiographic development of a watershed.
Groundwater plays an important role for socio-economic development of Comoro watershed in Timor Leste.
Source apportionment is critical for guiding development of efficient watershed nitrogen (N) pollution control measures.
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